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北京南苑−通县断裂北东段结构特征及第四纪活动性研究

牛文治 何付兵 刘振华 崔玉斌 白凌燕 王安国 张悦泽 曹萌萌 周捷铭

牛文治,何付兵,刘振华,等,2023. 北京南苑−通县断裂北东段结构特征及第四纪活动性研究[J]. 地质力学学报,29(6):879−887 doi: 10.12090/j.issn.1006-6616.2023032
引用本文: 牛文治,何付兵,刘振华,等,2023. 北京南苑−通县断裂北东段结构特征及第四纪活动性研究[J]. 地质力学学报,29(6):879−887 doi: 10.12090/j.issn.1006-6616.2023032
NIU W Z,HE F B,LIU Z H,et al.,2023. Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity[J]. Journal of Geomechanics,29(6):879−887 doi: 10.12090/j.issn.1006-6616.2023032
Citation: NIU W Z,HE F B,LIU Z H,et al.,2023. Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity[J]. Journal of Geomechanics,29(6):879−887 doi: 10.12090/j.issn.1006-6616.2023032

北京南苑−通县断裂北东段结构特征及第四纪活动性研究

doi: 10.12090/j.issn.1006-6616.2023032
基金项目: 北京市地质调查项目(PXM2018-158203-000014);北京市自然科学基金资助(8234070)
详细信息
    作者简介:

    牛文治(1990—),男,硕士,工程师,从事区域地质与城市地质工作。E-mail:nwzqq@126.com

    通讯作者:

    何付兵(1980—),男,博士,研究员,北京市区域地质与活动断裂调查。E-mail:hefubing14@126.com

  • 中图分类号: P642.27

Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity

Funds: This research is financially supported by the Beijing Geological Survey Project (Grant No. PXM2018-158203-000014) and the Fund of the Beijing Natural Science Foundation(Grant No.8234070)
  • 摘要: 南苑−通县断裂是北京凹陷与大兴凸起的边界断裂,也是1665年北京$ 6{\dfrac{1}{2}}$级地震的主要控震断裂,其活动性对北京市土地规划利用和地质灾害预测有着重要意义。文章通过高精度重力、纵波和横波地震综合物探剖面以及钻孔联合地质剖面探测方法,调查研究了南苑−通县断裂带北东段的几何特征及其活动性。研究结果显示,南苑−通县断裂经过通州区平家疃村后转为近东西向,倾向北,倾角56°~75°;北东段新生代活动呈正断层属性,推测上断点埋深约为21.6 m,为晚更新世活动断裂。文章论证了南苑−通县断裂北东段的活动时代与中段、南西段不同,为首都地区国土空间规划及防灾减灾体系建设提供了重要的地质依据。

     

  • 图  1  研究区地质构造简图

    F1—南口山前断裂;F2—黄庄−高丽营断裂;F3—顺义断裂;F4—南苑−通县断裂;F5—礼贤断裂;F6—夏垫断裂;F7—南口−孙河断裂;F8—二十里长山断裂;F9—永定河断裂;F10—桐柏断裂;F11—李桥断裂;F12—楼梓庄断裂;F13—西集断裂a—北京市平原区主要断裂分布图;b—南苑−通县断裂北东段断裂分布图及工作部署图

    Figure  1.  Schematic map of geological structure in the study area

    (a) Distribution map of major faults in the plain area of Beijing; (b) Distribution map and work deployment map of Nanyuan–Tongxian fault F1–Nankou piedmont fault; F2–Huangzhuang–Gaoliying fault; F3–Shunyi fault; F4–Nanyuan–tongxian fault; F5–Lixian fault; F6–Xiadian fault; F7–Nankou–Sunhe fault; F8–Ershilichangshan fault; F9–Yongdinghe fault; F10–Tongbai fault; F11–Liqiao fault; F12–Louzizhuang fault; F13–Xiji fault

    图  2  南苑−通县断裂北东段物探解译综合剖面图

    Figure  2.  Comprehensive profile of geophysical exploration and interpretation for the Northeast section of the Nanyuan–Tongxian fault

    图  3  钻孔联合地质剖面综合解释

    Figure  3.  Comprehensive interpretation map of composite drilling geological section

    表  1  碳十四样品测试结果一览表

    Table  1.   Test Results of 14C Samples

    样品编号岩性取样深度/m年龄/ka置信度
    ZK05–6.7 含有机质灰色黏土质粉砂6.711.84±0.0495.4%
    ZK06–10.1含有机质灰色黏土质粉砂10.122.62±0.0795.4%
    下载: 导出CSV

    表  2  光释光样品测试结果一览表

    Table  2.   Test results of OSL samples

    样品编号取样深度/m环境剂量率
    /(Gy/ka)
    等效剂量
    /Gy
    年龄/ka测试方法
    ZK04(16.0—16.2)16.0~16.23.04±0.13103.3±0.234.00±1.41SAR
    ZK07(16.8—17.0)16.8~17.03.15±0.13113.2±6.135.88±2.41SAR
    下载: 导出CSV
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  • 收稿日期:  2023-03-15
  • 修回日期:  2023-10-10
  • 预出版日期:  2024-01-02

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